Titlebook: Water and Plant Life; Problems and Modern O. L. Lange,L. Kappen,E.-D. Schulze Book 1976 Springer-Verlag Berlin · Heidelberg 1976 Plant phy

GLOOM

Soil Water Relations and Water Exchange of Forest Ecosystemsct. III. The combined form of these two laws allows in particular to determine the rates of water transfer within the soil and the corresponding rates of water storage or depletion. The application of the equation of continuity without sink or source terms implies that we have to deal with a constant total amount of recycling water.

Vaginismus

Keshan-disease

SPURN

The Soil-Plant-Atmosphere Continuume last century a prime interest focused on the mechanism of flow from roots to plant tops. This problem seems to have been solved by the cohesion theory, proposed and elaborated by B?hm (1893), Askenasy (1895), and Dixon and Joly (1895). The boldness that was originally necessary to propose such a t

Additive

The Soil-Plant-Atmosphere Continuume last century a prime interest focused on the mechanism of flow from roots to plant tops. This problem seems to have been solved by the cohesion theory, proposed and elaborated by B?hm (1893), Askenasy (1895), and Dixon and Joly (1895). The boldness that was originally necessary to propose such a t

CYN

The Water Status in the Plant Experimental Evidence. This leaves the task of providing quantitative data for at least some of the parameters discussed. The choice of these parameters and of the papers dealing with them has to be rather subjective, since even the most recent literature is far too voluminous to be covered completely.

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Hirsutism

方舟

Root Extension and Water Absorptionrtaken by texts such as Slatyer (1967) and Kramer (1969). Furthermore, various facets of the subject have been well covered in recent reviews by Weatherley (1970), Gardner (1968), Cowan and Milthorpe (1968), and particularly by Newman (1974). Characteristics of root growth, development, and senescen

Canary

Resistance to Water Flow in the Roots of Cerealsoil and high evaporative demand, supply often falls below demand and yield suffers. To extract water from the soil at a rate sufficient to match demand, gradients in water potential have to develop to overcome resistances to flow located in the soil and in the plant itself. This chapter deals with t